Dislocation creep in MgSiO3 perovskite at conditions of the Earth's uppermost lower mantle

@article{Cordier2004DislocationCI,
  title={Dislocation creep in MgSiO3 perovskite at conditions of the Earth's uppermost lower mantle},
  author={P. Cordier and T. Ung{\'a}r and L. Zsoldos and G. Tichy},
  journal={Nature},
  year={2004},
  volume={428},
  pages={837-840}
}
  • P. Cordier, T. Ungár, +1 author G. Tichy
  • Published 2004
  • Medicine, Materials Science
  • Nature
  • Seismic anisotropy provides an important observational constraint on flow in the Earth's deep interior. The quantitative interpretation of anisotropy, however, requires knowledge of the slip geometry of the constitutive minerals that are responsible for producing rock fabrics. The Earth's lower mantle is mostly composed of (Mg, Fe)SiO3 perovskite, but as MgSiO3 perovskite is not stable at high temperature under ambient pressure, it has not been possible to investigate its mechanical behaviour… CONTINUE READING

    Figures, Tables, and Topics from this paper.

    Postperovskite phase transition and its geophysical implications
    • 147
    • PDF

    References

    Publications referenced by this paper.
    SHOWING 1-10 OF 50 REFERENCES
    Deformation of (Mg0.9,Fe0.1)SiO3 Perovskite aggregates up to 32 GPa
    • 76